Illustrations of the Huttonian Theory of the EarthPlayfair, John
Science
Illustrations of the Huttonian Theory of the Earth
Playfair, John
Geology; Hutton, James, 1726-1797. Theory of the earth
316. The view thus afforded of the operations, in their nascent state,
which have shaped out and fashioned the present surface of the land,
is necessary to prepare us for following them to the utmost extent
of their effects. From these effects, the truth of the proposition,
that rivers have cut and formed, not the beds only, but the whole of
the valleys, or rather system of valleys, through which they flow, is
demonstrated on a principle which has a close affinity to that on which
chances are usually calculated, § 99. In order to conceive rightly the
course of a great river, and the communication subsisting between the
main trunk and its remotest branches, let us take the instance of the
Danube and cast our eyes on one of the maps constructed by MARSIGLI,
for illustrating the natural history of that great river.[163] When
it is considered, that over all the vast and uneven surface, which
reaches from the Alps to the Euxine, and from the mountains of Crapack
to those of Hæmus, a regular communication is kept up between every
point and the line of greatest depression, in which the river flows, no
one can hesitate to acknowledge, that it is the agency of the waters
alone which has opened them a free passage through all the intricacies
of this amazing labyrinth. In effect, suppose this communication to be
interrupted, and that some sudden operation of nature were to erect a
barrier of mountains to oppose the Theise or the Drave, as they rolled
their waters to the Danube. From this what could possibly result, but
the damming up of those rivers till their waters were deep, or high
enough to find a vent, either under the bases or over the tops of the
opposing ridge. Thus there would be formed immense lakes and immense
cataracts, which, by filling up what was too low, and cutting down what
was too high, would in time restore such a uniform declivity of surface
as had before prevailed. Just so in the times that are past, whatever
may have been the irregularities of the surface at its first emerging
from the sea, or whatever irregularities may have been produced in
it by subsequent convulsions, the slow action of the streams would
not fail in time to create or renew a system of valleys communicating
with one another, like that which we at present behold. Water, in all
circumstances, would find its way to the lowest point; though, where
the surface was quite irregular, it would not do so till after being
dammed up in a thousand lakes, or dashed in cataracts over a thousand
precipices. Where neither of these is the case; and where the lake and
the cataract are comparatively rare phenomena; there we perceive that
constitution of a surface, which water alone, of all physical agents,
has a tendency to produce; and we must conclude, that the probability
of such a constitution having arisen from another cause, is, to the
probability of its having arisen from the running of water, in such a
proportion as unity bears to a number infinitely great.
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